“…During the establishment of criticality the crust must be characterized by both susceptibility to external factors (WEI et al, 2000;XIA et al, 2002) and strong correlation between its different parts. The former will lead to triggering of earthquakes by tidal stress (GRASSO and SORNETTE, 1998) and consequently anomalously high values of LURR (YIN and YIN, 1991;YIN, 1993;YIN et al, 1994YIN et al, , 1995YIN et al, , 1996YIN et al, , 2000YIN et al, , 2002 are observed prior to large earthquakes. The latter will lead to establishment of long-range correlations in the regional stress field (SYKES and JAUME, 1990;RUNDLE et al, 1999;SAMMIS and SMITH, 1999;PLACE, 2000, 2002;WEATHERLEY, 2002) and accelerating seismic activity of moderate-sized earthquakes (ELLSWORTH et al, 1981;KEILIS-BOROK, 1990;SORNETTE and SAMMI;KNOPOFF et al, 1996 andBOWMAN et al, 1998) and equivalently, the accelerating seismic release prior to large earthquakes follows a power-law time-to-failure relation -AMR/AER (BUFE and VARNES, 1993;BOWMAN et al, 1998;JAUME and SYKES, 1999).…”